1887

Abstract

A stable method for calculating 3D-3C seismic reflected and transmitted wavefields in a horizontally layered anisotropic viscoelastic medium is derived. It makes use of delta-operators, the sixth-dimensional Stroh formalism and the Haskell-Thomson matrix

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/content/papers/10.3997/2214-4609.201400095
2009-06-08
2022-01-21
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400095
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